ClimateSearch

Lisala, Mongala

Democratic Republic of the Congo · 117k people · 415 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high90°F (32°C)90°F (32°C)88°F (31°C)87°F (30°C)86°F (30°C)85°F (29°C)84°F (29°C)83°F (29°C)84°F (29°C)83°F (29°C)84°F (29°C)87°F (30°C)
Average low73°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)72°F (22°C)73°F (23°C)
Dew point70°F (21°C)71°F (22°C)73°F (23°C)74°F (23°C)74°F (23°C)73°F (23°C)72°F (22°C)72°F (22°C)73°F (23°C)73°F (23°C)73°F (23°C)72°F (22°C)
Rainfall1.7 in (43 mm)2.7 in (69 mm)5.3 in (135 mm)5.6 in (141 mm)4.8 in (121 mm)4.4 in (112 mm)4.9 in (124 mm)6.4 in (163 mm)6.6 in (169 mm)7.6 in (194 mm)5.8 in (147 mm)2.4 in (61 mm)
Rainy days91218212120222625262312
Snowfall0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)
Sunshine328 h295 h309 h289 h298 h284 h290 h280 h274 h273 h272 h312 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+1.0°F (+0.6°C)

Models range from +0.5°F (+0.3°C) to +1.7°F (+0.9°C)

Days above 90°F (32°C) a year

49 76

About 1.5× as many

Warming by month
  • January: −0.4°F (−0.2°C)
  • February: +0.0°F (+0.0°C)
  • March: +1.1°F (+0.6°C)
  • April: +1.8°F (+1.0°C)
  • May: +2.2°F (+1.2°C)
  • June: +1.7°F (+0.9°C)
  • July: +0.8°F (+0.5°C)
  • August: +0.6°F (+0.3°C)
  • September: +0.8°F (+0.4°C)
  • October: +0.8°F (+0.5°C)
  • November: +0.7°F (+0.4°C)
  • December: +0.2°F (+0.1°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.